Concentration of elements or element groups in a geological body is the result of multiple stages of rockforming and ore-forming geological processes.An ore-forming element group can be identified by PCA(principal com...Concentration of elements or element groups in a geological body is the result of multiple stages of rockforming and ore-forming geological processes.An ore-forming element group can be identified by PCA(principal component analysis)and be separated into two components using BEMD(bi-dimensional empirical mode decomposition):(1)a high background component which represents the ore-forming background developed in rocks through various geological processes favorable for mineralization(i.e.magmatism,sedimentation and/or metamorphism);(2)the anomaly component which reflects the oreforming anomaly that is overprinted on the high background component developed during mineralization.Anomaly components are used to identify ore-finding targets more effectively than ore-forming element groups.Three steps of data analytical procedures are described in this paper;firstly,the application of PCA to establish the ore-forming element group;secondly,using BEMD on the o re-forming element group to identify the anomaly components created by different types of mineralization processes;and finally,identifying ore-finding targets based on the anomaly components.This method is applied to the Tengchong tin-polymetallic belt to delineate ore-finding targets,where four targets for Sn(W)and three targets for Pb-Zn-Ag-Fe polymetallic mineralization are identified and defined as new areas for further prospecting.It is shown that BEMD combined with PCA can be applied not only in extracting the anomaly component for delineating the ore-finding target,but also in extracting the residual component for identifying its high background zone favorable for mineralization from its oreforming element group.展开更多
The Nanling Range in South China is well known for its rich granite-related W–Sn deposits.To elucidate the controls of different granite-related W–Sn metallogenesis in the region,we chose five representative orerela...The Nanling Range in South China is well known for its rich granite-related W–Sn deposits.To elucidate the controls of different granite-related W–Sn metallogenesis in the region,we chose five representative orerelated granites(Yanbei,Mikengshan,Tieshanlong,Qianlishan,and Yaogangxian intrusions)in the Hunan–Jiangxi region,and studied their magmatic zircon ages and trace element geochemistry.Our new zircon data showed the differences in ages,temperatures and oxygen fugacity of the ore-forming magmas.Zircon U–Pb ages of the Yanbei and Mikengshan intrusions are characterized by 142.4±2.4 and 143.0±2.3 Ma,respectively,whereas the Tieshanlong and Qianlishan intrusions are 159.5±2.3and 153.2±3.3 Ma,respectively.The Sn-related intrusions were younger than the W-related intrusions.The Tiin-zircon thermometry showed that there was no systematic difference between the Sn-related Yanbei(680–744℃)and Mikengshan(697–763℃)intrusions and the W-related Tieshanlong(730–800℃),Qianlishan(690–755℃)and Yaogangxian(686–751℃)intrusions.However,the zircon Ce^4+/Ce^3+ratios of the Yanbei(averaged at 18.3)and Mikengshan(averaged at 18.8)intrusions are lower than those of the Tieshanlong(averaged at 36.9),Qianlishan(averaged at 38.4)and Yaogangxian(averaged at 37)intrusions,indicating that the Sn-related granitic magmas might have lower oxygen fugacities than those of the W-related.This can be explained by that,in more reduced magmas,Sn is more soluble than W and thus is more enriched in the residual melt to form Sn mineralization.The difference in source materials between the Sn-related and the W-related granites seems to have contributed to the different redox conditions of the melts.展开更多
2016年10月30日下午,美国EB-5投资移民—费城喜达屋W/Elment酒店项目发布会在中国大饭店宴会厅举行。该发布会由United Lead主办,汇通基金承办。费城资深政要Jack Ferguson,酒店资深分析家Peter Raymond Tyson,项目执行总裁Andrew Stuar...2016年10月30日下午,美国EB-5投资移民—费城喜达屋W/Elment酒店项目发布会在中国大饭店宴会厅举行。该发布会由United Lead主办,汇通基金承办。费城资深政要Jack Ferguson,酒店资深分析家Peter Raymond Tyson,项目执行总裁Andrew Stuart Gibbs作为特邀嘉宾出席了发布会。众多美国投资移民界的贵宾与United Lead高层齐聚一堂,为到场嘉宾奉上一场最顶级的美国EB-5投资移民项目全解析。展开更多
通过对两种成分单晶镍基合金进行蠕变曲线测定,长期时效处理及组织形貌观察,研究了元素W含量对单晶合金组织与性能的影响。结果表明:在N i-A l-Cr-Ta-Co-x%W-5.5%Mo系单晶合金中,4wt%W合金在982℃,200MPa条件下,具有较长的蠕变寿命,随W...通过对两种成分单晶镍基合金进行蠕变曲线测定,长期时效处理及组织形貌观察,研究了元素W含量对单晶合金组织与性能的影响。结果表明:在N i-A l-Cr-Ta-Co-x%W-5.5%Mo系单晶合金中,4wt%W合金在982℃,200MPa条件下,具有较长的蠕变寿命,随W含量增加到6wt%,合金的蠕变寿命明显降低。高W合金在有/无应力时效期间,析出针状μ相,使合金基体出现难溶元素的贫化区,是导致合金蠕变寿命降低的主要原因。其中μ相在(001)晶面沿<110>方向呈相互平行、或垂直的针状形貌析出,沿{111}晶面呈片状方式生长,且与γ′相相邻。展开更多
基金funded by the Na-tional Natural Science Foundation of China(Grant Nos.41672329,41272365)the National Key Research and Development Project of China(Grant No.2016YFC0600509)the Project of China Geological Survey(Grant No.1212011120341)
文摘Concentration of elements or element groups in a geological body is the result of multiple stages of rockforming and ore-forming geological processes.An ore-forming element group can be identified by PCA(principal component analysis)and be separated into two components using BEMD(bi-dimensional empirical mode decomposition):(1)a high background component which represents the ore-forming background developed in rocks through various geological processes favorable for mineralization(i.e.magmatism,sedimentation and/or metamorphism);(2)the anomaly component which reflects the oreforming anomaly that is overprinted on the high background component developed during mineralization.Anomaly components are used to identify ore-finding targets more effectively than ore-forming element groups.Three steps of data analytical procedures are described in this paper;firstly,the application of PCA to establish the ore-forming element group;secondly,using BEMD on the o re-forming element group to identify the anomaly components created by different types of mineralization processes;and finally,identifying ore-finding targets based on the anomaly components.This method is applied to the Tengchong tin-polymetallic belt to delineate ore-finding targets,where four targets for Sn(W)and three targets for Pb-Zn-Ag-Fe polymetallic mineralization are identified and defined as new areas for further prospecting.It is shown that BEMD combined with PCA can be applied not only in extracting the anomaly component for delineating the ore-finding target,but also in extracting the residual component for identifying its high background zone favorable for mineralization from its oreforming element group.
基金supported by the National Basic Research Program of China (973 Program) (Grants No. 2014CB440906)Innovation Team Program of Chinese Academy of Sciences (Overseas Famous Scholars Program)‘‘Light of West China’’ Program of Chinese Academy of Sciences
文摘The Nanling Range in South China is well known for its rich granite-related W–Sn deposits.To elucidate the controls of different granite-related W–Sn metallogenesis in the region,we chose five representative orerelated granites(Yanbei,Mikengshan,Tieshanlong,Qianlishan,and Yaogangxian intrusions)in the Hunan–Jiangxi region,and studied their magmatic zircon ages and trace element geochemistry.Our new zircon data showed the differences in ages,temperatures and oxygen fugacity of the ore-forming magmas.Zircon U–Pb ages of the Yanbei and Mikengshan intrusions are characterized by 142.4±2.4 and 143.0±2.3 Ma,respectively,whereas the Tieshanlong and Qianlishan intrusions are 159.5±2.3and 153.2±3.3 Ma,respectively.The Sn-related intrusions were younger than the W-related intrusions.The Tiin-zircon thermometry showed that there was no systematic difference between the Sn-related Yanbei(680–744℃)and Mikengshan(697–763℃)intrusions and the W-related Tieshanlong(730–800℃),Qianlishan(690–755℃)and Yaogangxian(686–751℃)intrusions.However,the zircon Ce^4+/Ce^3+ratios of the Yanbei(averaged at 18.3)and Mikengshan(averaged at 18.8)intrusions are lower than those of the Tieshanlong(averaged at 36.9),Qianlishan(averaged at 38.4)and Yaogangxian(averaged at 37)intrusions,indicating that the Sn-related granitic magmas might have lower oxygen fugacities than those of the W-related.This can be explained by that,in more reduced magmas,Sn is more soluble than W and thus is more enriched in the residual melt to form Sn mineralization.The difference in source materials between the Sn-related and the W-related granites seems to have contributed to the different redox conditions of the melts.
文摘2016年10月30日下午,美国EB-5投资移民—费城喜达屋W/Elment酒店项目发布会在中国大饭店宴会厅举行。该发布会由United Lead主办,汇通基金承办。费城资深政要Jack Ferguson,酒店资深分析家Peter Raymond Tyson,项目执行总裁Andrew Stuart Gibbs作为特邀嘉宾出席了发布会。众多美国投资移民界的贵宾与United Lead高层齐聚一堂,为到场嘉宾奉上一场最顶级的美国EB-5投资移民项目全解析。
文摘通过对两种成分单晶镍基合金进行蠕变曲线测定,长期时效处理及组织形貌观察,研究了元素W含量对单晶合金组织与性能的影响。结果表明:在N i-A l-Cr-Ta-Co-x%W-5.5%Mo系单晶合金中,4wt%W合金在982℃,200MPa条件下,具有较长的蠕变寿命,随W含量增加到6wt%,合金的蠕变寿命明显降低。高W合金在有/无应力时效期间,析出针状μ相,使合金基体出现难溶元素的贫化区,是导致合金蠕变寿命降低的主要原因。其中μ相在(001)晶面沿<110>方向呈相互平行、或垂直的针状形貌析出,沿{111}晶面呈片状方式生长,且与γ′相相邻。
